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WU Meiren, CHEN Qi, WANG Xianguang, CHEN Guohua, WAN Haozhang, YAN Jiayong, OUYANG Yongpeng. 2019. Geochemistry and petrogenesis of the Zaolin basanite in the northeastern Jiangxi Province[J]. Geology in China, 46(4): 850-860. doi: 10.12029/gc20190415
Citation: WU Meiren, CHEN Qi, WANG Xianguang, CHEN Guohua, WAN Haozhang, YAN Jiayong, OUYANG Yongpeng. 2019. Geochemistry and petrogenesis of the Zaolin basanite in the northeastern Jiangxi Province[J]. Geology in China, 46(4): 850-860. doi: 10.12029/gc20190415
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Geochemistry and petrogenesis of the Zaolin basanite in the northeastern Jiangxi Province

  • 1.

    No. 912 Geological Surveying Party, Jiangxi Bureau of Geology and Mineral Exploration and Development, Yingtan 335001, Jiangxi, China

  • 2.

    Administration of Geological Exploration of Jiangxi Province, Nanchang 330025, Jiangxi, China

  • 3.

    China Deep Exploration Center-SinoProbe Center, Chinese Academy of Geological Sciences, Beijing 100037, China

    • Fund Project: Supported by China Geological Survey Program (No. 121201103000150017, 12120113065300, DD20160346, DD20160082, DD20190012), Jiangxi Provincial Geological Exploration Fund Management Center (No. [2015]00-13), Welfare Research Program of Ministry of Land and Resources (No. 201411035), and Jiangxi Geological and Mineral Exploration and Development Bureau Foundation (No. JGMEDB [2017]78)
More Information
  • Author Bio: WU Meiren, male, born in 1966, senior engineer, mainly engages in geological prospecting and research; E-mail:1067992037@qq.com
  • Corresponding author: OUYANG Yongpeng, male, born in 1988, master, engineer, mainly engages in geological exploration; E-mail:yongpeng0524@163.com
Received Date:  10 January 2019
Revised Date:  25 June 2019
Publish Date:  25 August 2019
    Abstract

  • Two Cenozoic basanite dykes were newly discovered in the Zhuxi ore-concentration area, northeastern Jiangxi Province, eastern China. They have high SiO2 (41.08%-42.94%), Na2O+K2O (4.95%-6.30%), TiO2 (2.19%-2.43%) contents, and high Mg# (0.61 -0.65). Geochemistry characteristics of these basanite dykes show they are enriched in Nb, Ta, Th, Zr, Ni, Cr, Sc, while depleted in Ba, Ti, K, and P. Their ∑REE values are from 299.16×10-6 to 375.00×10-6% with LREE/HREE ratios of 5.45-6.71 and δEu values of 0.88 to 0.94. According to the geochemical discrimination diagrams and the ratios of incompatible elements, we suggest that the basanite dykes were derived from partial melting of garnet forsterite (0.2%-0.5%) and herzolite (0.5%-1%), which may be caused by upwelling of carbonate melt in the asthenosphere mantle in response of the subduction of the Paleo-Pacific Ocean.

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